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What we build on: The hidden history of the soils and cadavers under Bascom hill.

What We Build On
It was a brisk October day. My breath hung in the air. Tourists huddled around me with their hands wedged tightly in their coat pockets, and they breathed into the cold with pursed lips. We stood there, feet grounded on the marble bricks outside the Historical Society. Our tour leader greeted us. Frosty air rippled out in smoky chains from her mouth as she spoke. “Shall we begin?” she asked. We smiled, mumbling our agreements, and began our historical tour of Bascom. Bascom Hall, and the Hill it sits on, has represented the regality of the University of Wisconsin campus since its construction in 1857[1], but many forget about the history beneath the hill. This is a story of the silent, the overlooked—the invisible. This is a story of soil. This is a story of what we build on
We made our strides in long lunges as we hoisted our bodies up Bascom Hill. This was a story my legs understood. This was a story of great energy. Roughly 18,000 years ago, the University of Wisconsin campus was covered by a glacier; the same glacier that gave this area its famous four lakes[2]. This monstrous slab of ice shaped and deposited sand and gravel as its mass sloughed off and receded. Bascom Hill is a glacial drumlin, and drumlins are historical compasses. They point to the direction of glacial recession[3]. The long hill of Bascom runs east to west and points to the eastward recession of the glacier thousands of years ago. Figure 1 is a reconstruction of the glacial flow in Wisconsin, and shows the east-west direction of ice flow near Dane County. This colossal glacier left the rocky pile of parent material my legs were ascending that day, but they also shaped the soils beneath my feet.



Figure 1: Reconstruction of Glacial Ice Flow in Wisconsin.[4]
As we ascended the hill we were oblivious to the change in soil as we climbed. As our boot heels clanked on the marble slabs outside the historical society where our journey began, they compressed, ever so slightly, the fertile organic histosol soils underneath them[5]. Histosol soils are oxygen deprived, which makes them incredibly productive for farming. Oxygen normally aids in the breakdown of organic material, and the absence of oxygen causes a thick organic hummus layer to form on the top of the soil[6]. This oxygen restriction came from years of waterlogged soils, reminding us that Madison was once covered in a menagerie of wetlands[7]. As we ascended, the soils changed to dryer less fertile soils on top the glacial drumlin we know as Bascom. The rocky elevated landscape left by the glacier made these soils immune from the effects of waterlogging for thousands of years[8]. We slowed down and caught our breath at the feet of Abe Lincoln, where our tour guide pointed out two modest tombstones, a few square inches each in size.

Figure 2: Gravestones near Abe Lincoln on Bascom[9]
 My feet became uneasy with the possibility of what, or whom, they were compressing at that moment. Our tour guide told us the story of two men, Samuel Warren (S.W.) and William Nelson (W.N.)—who were accidentally exhumed from Bascom during the transplant of Abe Lincoln in 1918[10]. Bascom Hill was used as burial site by the German and English settlers in the early 1800's, and these two men were unlucky enough to be caught under the shovels of the excavators. The cadavers were reburied under the feet of Abe Lincoln, and were forgotten under the soil. Samuel and William were not the only bodies forgotten under the soil in Bascom however.
Before Bascom was delicately smoothed over by the university, the hill was originally "tangle of blackberry bushes frequented by bears and rattlesnakes" as documented by pioneer woman Rosalina Peck in 1837[11]. This landscape was made rough by the vegetation, but also had a rough, uneven surface. The original uneven surface would not only be the mark of nature’s chaotic tendencies, but also the intent of humans.
Prior to (and after) European settlement of the Madison region, Ho-Chunk Indians (also referred to as Winnebago) lived on the fertile wetlands surrounding the five lakes[12]. These lakes would have been a life giving presence for the native populations, and they treated them as such. It was Ho-Chunk belief that a water-panther spirit resided in Lake Mendota. In honor of this water spirit, the Ho-Chunk built a burial mound in the shape of a panther on the Bascom Hill[13]. It was this memorial mound that was smoothed over to make the hill the sloping giant it is today. 




Figure 3: Sign of campaign to ‘fill the hill’[14].
Bascom Hall has long been cherished for years as a place of tradition and community at the university. As we walked, we passed charity signs for UW donations that marched up with us along the hill, but this time they felt much more ominous and satirical. “Share the hill!” they proclaimed. “Fill the hill!” shouted another (Figure 3). What they meant, was, to fill the hill with pink flamingos that represented donations to the university, but knowing what the hill was actually filled with added a melancholy reminder of  our deep, fostered ignorance of the history of the hill. I lingered on this thought as my legs made the last contractions up Bascom Hill. Step 1. Step 2. Step 3. We turned around to view the beautiful cityscape.

Figure 3: View from Bascom[15]
The view from Bascom is a beautiful, symmetrical world of brick and concrete. The nature contained there is tightly manicured for visual aesthetic. But these manicured trees and plants remind us of the potential under the concrete. These trees remind us of the life in the soils we have covered and tunneled under--the land that the city obscures.
In 1850, the fertile histosol soils of the Madison lowlands were not paved over, but were farmed. Figure 4 shows a similar view of the city from Bascom, but in this painting we see a much different landscape. It wove the pastoral and the urban. In Figure 5 a farmhouse sits on the main road. The fence surrounding this house suggests the land was used for farming or grazing. This farm’s close proximity to the road indicates a need for fast travel of time-precious meat, milk or vegetables for transport; goods that were probably locally produced and consumed. It was not completely out of choice that this patchwork of landscapes existed in the same place, but
also necessity.

Figure 4: View of Capitol from Bascom area in 1865[16]


Figure 5: View of Bascom and Surrounding Farms (1865)[17]
Transportation affected how people and goods moved in Madison. During 1865, residents got around the city by foot or by horse and buggy. In Figure 4 the wide streets are carved with ruts from wagon wheels that traveled through the city. The road in Figure 5 is likely also a wagon road. While horse and buggy worked for much of the local transportation, long distance travel became available through Madison’s Rail system (Figure 6). While this rail system initially only connected Madison and nearby Watertown, it later would grow and deepen Madison’s ability to use distant trade for its sustenance.



Figure 6: Map of Madison-Watertown Rail 1857[18]
As railroad and automotive technologies grew, the city was able to become more and more reliant upon shipped goods. This allowed the city to grow onto the rural landscape, which in return deepened its dependence on imports.  Today, the University’s cityscape is a reminder of our dependence of outside markets. The farm houses in Figure 5 and the fertile soils they rested on are now completely obscured with city buildings and houses, presupposing an ability to live without local farmland. The view now reminds us of the history of campus, but silences our understanding of our ecological relationship to the soil. As we looked out over this world of brick and concrete, we saw the crown of the capitol building peaking out over the horizon.
Our tour guide pointed her finger over to the capitol. The building has the same Greco-Roman style as Bascom. This represents not only the period of Greek revival during the mid-1800’s when both buildings were originally built[19], but the intended conversation between the two buildings. Their marble crown tops and columned mouths watch at each other across State Street. They are able to ‘see’ each other because they sit atop hills that overlook Madison—physically and metaphorically representing the two great superpowers in Madison.
“There was not originally a hill at the capitol building” our tour guide began. “They used dirt from around the area to build the hill”. I thought about the intended conversation even more. The state set out to make these two buildings talk, even if the hills they sat on needed to be fabricated to talk to allow it. “Where do you think they got the dirt?” She asked. We looked at her, not knowing, or not wanting to know, the answer to her rhetorical question. “From the burial mounds surrounding the area!” she exclaimed. A deep discomfort knotted inside me.
The tour was a haunted tour of Madison, but it was not the ghosts or the dead that haunted me. It was my complete ignorance of them—of the history hidden beneath my feet. I could not help but think of the Capitol Building and Bascom compressing the organic compost of bodies down into the soil. I could not help but to think of the cadavers, the culture, and the history of the Ho-Chunk Indians we paved over for this campus. I was not haunted by apparitions, for it was not my ability to see these people that haunted me, it was my complete oblivion to them that scared me most.  Now as I look up at the regal height of Bascom, I do not only see the story of the university. I see the stories of the silent, the overlooked and the invisible. I see the stories of the soil. I see what we build on.


References
Barber, John and Howe, Henry. Authors. “The Loyal West in the Times of the Rebellion”.  Photograph. From Wikipedia Commons. http://en.wikipedia.org/wiki/File:Madison_WI_Barber_1865p439cropped.jpg#filehistory. (Accessed September 23, 2013)
Bennett, Matthew, and Neil F. Glasser. Glacial geology: ice sheets and landforms. 2nd ed. Chichester, UK: Wiley-Blackwell, 2009.
Birmingham, Robert A., and Katherine H. Rankin. Native American mounds in Madison and Dane County. Madison, Wis.: City of Madison and the Native American Center, 1994.
Colton, J. H. Author. Watertown and Madison RR. Print. From Wisconsin Historical Society. http://preview.wisconsinhistory.org/Content.aspx?dsNav=Ny:True,Nrc:id-4294966726,N:4294963828-4294955414&dsNavOnly=Ny:True,N:4294966724&dsRecordDetails=R:IM90122 (Accessed September 23, 2013)
David, Mickelson. "Who knew?." (Dec. 12, 2000). http://www.news.wisc.edu/5643 (accessed November 18, 2013).

Fuller, John S, Photographer. [First Three Buildings on the University of Wisconsin-Madison Campus] Photograph. From Wisconsin Historical Society Fuller, John S., 1815-1902 : Madison, Wisconsin, cartes-de-visite, ca. 1860-ca. 1870. http://preview.wisconsinhistory.org/Content.aspx?dsNav=Ny:True,Nrc:id-4294966726,N:4294963828-4294955414&dsNavOnly=Ny:True,N:4294966724&dsRecordDetails=R:IM1885 (Accessed September 23, 2013)

General Land Office. Plat Map Sketch of Madison Area. Dec 1834. Wisconsin Historical Society. http://digicoll.library.wisc.edu/cgi-bin/SurveyNotes/SurveyNotes-idx?type=article&dtype=Sketch+Map&twp=T007NR009E
Natural Resources Conservation Service. "Histosols." NRCS Soils. http://soils.usda.gov/technical/classification/orders/histosols.html (accessed November 19, 2013).
Kondreck, Robert , Zelenda Koch, and Jim Gutkowski. "Wisconsin Galciation as seen in Jefferson County: The Hausz Brothers Quarry." Wisconsin Galciation as seen in Jefferson County: The Hausz Brothers Quarry. http://www4.uwm.edu/letsci/geosciences/trips_tours/ugfc/wi_glaciation/WI_glaciation.html (accessed November 18, 2013).
Rath, Jay. "Bascom Hill: Old haunt or still haunted?." Wisconsin State Journal, October 24, 1988.
Rath, Jay. "The Haunting of Bascom Hill." Madison Magazine, September 1992.
Silverman, Claire. “Evolving from Indian mounds to flamingos” The Herald, May 7, 1983.
University of Wisconsin. "Bascom Hall." Wisc.edu. http://www2.fpm.wisc.edu/ppnew/featurebldg/pdf/bascom.pdf (accessed November 24, 2013).





[1] University of Wisconsin "Bascom Hall." Wisc.edu. University of Wisconsin, n.d. Web. 24 Nov. 2013. http://www2.fpm.wisc.edu/ppnew/featurebldg/pdf/bascom.pdf.
[2] Mickelson, David. [Interview] Who Knew? (2000) http://www.news.wisc.edu/5643 (accessed November 18, 2013).
[4] Kondreck, Robert. Koch, Zelenda. Gutkowski, Jim. “Wisconsin Glaciation as seen in Jefferson County: The Hausz Brothers Quary”
[5] See Appendix images 2 and 3 for detailed maps describing the area’s soils.
[7] General Land Office. Plat Map Sketch of Madison Area. Dec 1834. Wisconsin Historical Society. http://digicoll.library.wisc.edu/cgi-bin/SurveyNotes/SurveyNotes-idx?type=article&dtype=Sketch+Map&twp=T007NR009E (photo of map in appendix, item 1)
[8] These effects can be seen by comparing the percentage of organic matter across the soils. One can see on the topographical map of Madison that the areas of high altitude also tend to be areas of low organic matter. In particular, there was a fertile cresent of delicate organic rich soils that swept southward from lake Monona, with 90 percent organic matter contained within them.
[9] Bascom Tombstones. Personal photograph by author. November 2013.
[11] Silverman, Claire. “Evolving from Indian mounds to flamingos” The Herald, May 7, 1983.
[12] Birmingham, Robert A., and Katherine H. Rankin. Native American mounds in Madison and Dane County. Madison, Wis.: City of Madison and the Native American Center, 1994. http://www.wisconsinhistory.org/madison/madisonmounds.pdf
[13] Silverman, Claire. “Evolving from Indian mounds to flamingos” The Herald, May 7, 1983.
[14] “Fill the Hill” Personal photograph by author. November 2013.
[15] View from Bascom. Personal photograph by author. September 2013.
[16] Barber, John and Howe, Henry. Authors. “The Loyal West in the Times of the Rebellion”.  Photograph. From Wikipedia Commons. http://en.wikipedia.org/wiki/File:Madison_WI_Barber_1865p439cropped.jpg#filehistory. (Accessed September 23, 2013)

[17]  Fuller, John S, Photographer. [First Three Buildings on the University of Wisconsin-Madison Campus] Photograph. From Wisconsin Historical Society Fuller, John S., 1815-1902 : Madison, Wisconsin, cartes-de-visite, ca. 1860-ca. 1870. http://preview.wisconsinhistory.org/Content.aspx?dsNav=Ny:True,Nrc:id-4294966726,N:4294963828-4294955414&dsNavOnly=Ny:True,N:4294966724&dsRecordDetails=R:IM1885 (Accessed September 23, 2013)


[18] Colton, J. H. Author. Watertown and Madison RR. Print. From Wisconsin Historical Society. http://preview.wisconsinhistory.org/Content.aspx?dsNav=Ny:True,Nrc:id-4294966726,N:4294963828-4294955414&dsNavOnly=Ny:True,N:4294966724&dsRecordDetails=R:IM90122 (Accessed September 23, 2013)
[19] Although both the capitol and Bascom have gone through renovations and rebuilding. 

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